CAJ | 학술논문

通过地震及钻孔资料对南海北部珠江口盆地重力流及等深流沉积进行了研究。南海北部重力流及等深流沉积类型多样，包括峡谷、单向迁移水道、堤岸、朵叶及漂积体。单向迁移水道迁移方向分别为北东向和南西西向，为重力流与等深流交互作用形成。漂积体有大型长条状漂积体、限制型漂积体和陆坡席状漂积体，岩性为粘土、泥质粉沙。南海北部陆坡水深200～1200m 范围内发育北东向迁移水道及小规模的漂积体，而水深约1200～3000m 内则以朵叶及大规模的漂积体为主，见少量南西西向迁移水道。其中，漂积体多分布于峡谷、水道及朵叶的两侧，为等深流改造堤岸、朵叶等“细粒”沉积物而成。
통과지진급찬공자료대남해북부주강구분지중력류급등심류침적진행료연구。남해북부중력류급등심류침적류형다양，포괄협곡、단향천이수도、제안、타협급표적체。단향천이수도천이방향분별위북동향화남서서향，위중력류여등심류교호작용형성。표적체유대형장조상표적체、한제형표적체화륙파석상표적체，암성위점토、니질분사。남해북부륙파수심200～1200m 범위내발육북동향천이수도급소규모적표적체，이수심약1200～3000m 내칙이타협급대규모적표적체위주，견소량남서서향천이수도。기중，표적체다분포우협곡、수도급타협적량측，위등심류개조제안、타협등“세립”침적물이성。
Using integrations of seismic data and core data,interactions between down-slope and along-slope processes had been studied.Gravity flow deposits and contourites are well developed in northern South China Sea,including canyon,unidirectionally migrational channels,levees,lobes,drifts and so on. Unidirectionally migrating channels result from interactions between gravity flow and contour current with migrating directions are northeast (NE)and west-southwest (WSW),respectively.Drifts consisted of clay and muddy silt could be divided into giant elongated,confined and slope sheeted drifts.NE-migrating channels and drifts are widespread at water depths of 200 m to 1 200 m.By contrast,lobes,drifts and few WSW-migrating are developed at depths of 1 200 m to 3 000 m.Contourites distribute on the both sides of canyon,channel and lobe,which result from reworking the fine-grained deposits of gravity flow.